the central Okinawa Trough 冲绳海槽中部
the northern okinawa trough 冲绳海槽北部
the south of okinawa trough 冲绳海槽南部
The magmatism in the Okinawa Trough contributed a lot to the hydrothermal activity not only as heat source but also as material source.
冲绳海槽的岩浆作用不仅为现代海底热液活动提供了热源，而且有气液相的物质供应。
参考来源 - 冲绳海槽火山岩中岩浆包裹体及气体同位素组成研究·2,447,543篇论文数据，部分数据来源于NoteExpress
The Okinawa Trough is a back arc basin still driven by the converging asthenosphere.
冲绳海槽仍是一个软流圈在汇聚的弧后盆地。
Finally, we get the 3d horizontal slice and the 2d profile of density imaging in the Okinawa Trough.
最后得到了冲绳海槽地区3d密度成像水平切片和2d密度成像剖面。
These results have provided important clues for understanding the extension history of the Okinawa Trough.
计算的结果为认识冲绳海槽拉张史提供了重要的线索。
应用推荐